What is Anabatic Wind?
Local winds that blow from slopes to peaks as a result of the heating of the top slopes without being affected by general pressure changes. Generally, the term is used for upward air currents, vertical movements in the formation of cumulus clouds, and valley breezes rather than anabatic winds. Anabatic winds are less common than katabatic winds, which occur through the opposite process.
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A bomb cyclone is a large mid-latitude storm that forms when a storm’s central pressure drops (i.e. “bombs out”), resulting...
A large body of air having similar horizontal temperature and moisture characteristics.
A sudden and rapid flow of snow masses accumulated on the slopes of mountainous areas under the influence of gravity or a...
A condition in which the stratification of the atmosphere depends on both air temperature and pressure, and where surfaces...
A low-pressure area with converging winds, rotating counterclockwise in the Northern Hemisphere and clockwise in the Southern...
A prefix used in cloud nomenclature to describe middle-altitude clouds that form between 6,500 and 20,000 feet, such as altostratus...
A tropical cyclone with sustained winds of at least 74 miles per hour, characterized by a central eye, strong winds, and...
A weather system refers to the movement of warm and cold air across the globe, usually in a recurring pattern. Systems can...
A cold core low is a low-pressure system where the coldest temperatures are found near the center. These systems are often...
The decrease in temperature with height in an adiabatically rising air parcel (lapse rate). For dry air, this value is 1...

